通过计算机模拟预测四氢呋喃水合物的单变量两相共存线。

J. Algaba, C. Romero-Guzmán, Miguel J Torrejón, F. J. Blas
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引用次数: 0

摘要

在这项研究中,通过分子动力学模拟确定了四氢呋喃(THF)水合物在 100 至 1000 巴范围内的单变量两相共存线。这项研究是通过将四氢呋喃水合物相与化学计量水溶液相接触来进行的。按照直接共存技术,压力是固定的,通过分析水合物相在不同温度值下是增长还是熔化来确定共存线。我们使用著名的 TIP4P/Ice 模型来描述水。我们使用了基于相平衡可转移参数-联合原子法(TraPPE-UA)的两种不同的 THF 模型,即原始(柔性)TraPPe-UA 模型及其刚性和平面版本。总体而言,在高压条件下,两种模型得出的结果差异很小。然而,使用这两种模型进行模拟所需的计算量却有很大差异,其中刚性平面模型的计算量要比原始模型快得多。我们还使用刚性和平面 THF 模型分析了在 250 bar 条件下水和 THF 分子之间不同的分散相互作用的影响。特别是,我们通过参数ξO-THF 修改了贝特洛组合规则,该参数可控制水-THF 的异色散相互作用。我们分析了当ξO-THF 从 1.0(原始贝特洛结合规则)修改为 1.4(修改后的贝特洛结合规则)时对水合物解离温度的影响。我们使用优化值 ξO-THF = 1.4 和刚性 THF 模型,以可转换的方式预测其他压力下的解离温度。我们发现计算机模拟预测与文献中的实验数据非常吻合。
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Prediction of the univariant two-phase coexistence line of the tetrahydrofuran hydrate from computer simulation.
In this work, the univariant two-phase coexistence line of the tetrahydrofuran (THF) hydrate is determined from 100 to 1000 bar by molecular dynamics simulations. This study is carried out by putting in contact a THF hydrate phase with a stoichiometric aqueous solution phase. Following the direct coexistence technique, the pressure is fixed, and the coexistence line is determined by analyzing if the hydrate phase grows or melts at different values of temperature. Water is described using the well-known TIP4P/Ice model. We have used two different models of THF based on the transferable parameters for phase equilibria-united atom approach (TraPPE-UA), the original (flexible) TraPPe-UA model and a rigid and planar version of it. Overall, at high pressures, small differences are observed in the results obtained by both models. However, large differences are observed in the computational efforts required by the simulations performed using both models, being the rigid and planar version much faster than the original one. The effect of the unlike dispersive interactions between the water and THF molecules is also analyzed at 250 bar using the rigid and planar THF model. In particular, we modify the Berthelot combining rule via a parameter ξO-THF that controls the unlike water-THF dispersive interactions. We analyze the effect on the dissociation temperature of the hydrate when ξO-THF is modified from 1.0 (original Berthelot combining rule) to 1.4 (modified Berthelot combining rule). We use the optimized value ξO-THF = 1.4 and the rigid THF model in a transferable way to predict the dissociation temperatures at other pressures. We find excellent agreement between computer simulation predictions and experimental data taken from the literature.
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